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INTO THE DEEP Competition Manual
Quiz by Wave Droids
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How many points do you score for placing an alliance-specific specimen in your low basket?
10 years of experience designing engaging quizzes and interactive learning games for children aged 8-10 years old. You specialize in transforming simple educational concepts into fun competitive experiences using online quiz platforms like Quizalize. Objective: Design a complete interactive multiplication quiz for third-grade students (8â9 years old) on the Quizalize platform. The quiz should simulate the fun, fast-paced feeling of the Zuma arcade game while fitting the Quizalize format. The aim is to help students practice multiplication tables (1Ă1 to 12Ă12) in an exciting, motivating, and competitive environment. Instructions: Structure: Design at least 40 multiplication questions. Questions should appear in increasing difficulty: start from easy (e.g., 2Ă3, 4Ă2) and move to harder problems (e.g., 11Ă12, 9Ă8). Timing: Set a short time limit for each question (e.g., 10 seconds) to simulate the fast reaction needed in Zuma. Encourage fast thinking and rapid response under time pressure. Answer Choices: Use multiple-choice answers. Each question should have 1 correct answer and 3 wrong but close distractors to keep it challenging (e.g., for 7Ă6: options 42, 43, 36, 48). Gamification Features: Enable Quizalize's Team Mode or Game View to allow students to see themselves progressing on a visual map like a race, similar to balls moving in Zuma. Set points bonuses for speed and accuracy. Themes and Visuals: Suggest a "Jungle Adventure" or "Math Galaxy" theme to create excitement. Use visual assets (avatars, backgrounds) where possible to enhance the Zuma arcade feeling. Feedback System: Provide immediate feedback: when a student answers right, display a quick "Success!" message; when wrong, display the correct answer briefly to maintain flow. Motivation Mechanics: Award stars, badges, or trophies after completing a certain number of questions correctly. Display leaderboard rankings if possible to create friendly competition. Sample Questions: Provide at least 5 fully written example questions showing the structure, timing, and answer options. Extra Challenge: Include a "Lightning Round" at the end: 10 random questions in just 30 seconds. Important: Keep language child-friendly and motivational. Make sure no question looks too similar to the others to avoid boredom. Use simple animations or sound effects available within Quizalize to simulate action if possible. Take a deep breath and work on this problem step-by-step.Subducting seafloor would lower the melting temperature of the mantle, generating magma that rises to the surface. What happens after magma is formed? Magma cools and crystallizes to form igneous rock. Igneous rock undergoes weathering (or breakdown) to form sediment.... As the sedimentary rock is buried under more and more sediment, the heat and pressure of burial cause metamorphism to occur. This transforms the sedimentary rock into a metamorphic rock. How Do Volcanoes Erupt? Deep within the Earth it is so hot that some rocks slowly melt and become a thick flowing substance called magma. Since it is lighter than the solid rock around it, magma rises and collects in magma chambers. Eventually, some of the magma pushes through vents and fissures to the Earth's surface. Magma that has erupted is called lava. Some volcanic eruptions are explosive and others are not. The explosivity of an eruption depends on the composition of the magma. If magma is thin and runny, gases can escape easily from it. When this type of magma erupts, it flows out of the volcano. A good example is the eruptions at Hawaii's volcanoes. Lava flows rarely kill people because they move slowly enough for people to get out of their way. If magma is thick and sticky, gases cannot escape easily. Pressure builds up until the gases escape violentlyInto The Sea Mary is a scientist. She studies plants and animals of the sea. She uses this little sub. It is a special sub that can dive deep into the water. The sub has tanks of air for her to breathe. The sub has bright lights, too. They help her see the plants. Mangrove and animals. She wants to see what kind of sharks live here. This sub has a camera. So she can take pictures of the sharks that swim by. Sometimes she dives off a boat into the sea. She puts on a special suit for diving. She wears an air tank. She wears a mask and flippers, too. She carries a special camera that works underwater. She takes pictures of the seaweed. She wants to see how big it can grow.A seed grows A small seed falls to the ground and becomes buried in the soft soil. The seed is buried in the soft soil, and the rain falls. The rain soaks into the soil that holds the small seed. The small seed soaks up water from the rain. The water feeds the seed, and roots grow down deep into the soil. The leaves and a stem grow up through the ground. The leaves gather in the sunshine. The plant uses sunshine to make food. The rain and the soil feed the small plant. The plant grows taller, and more leaves grow on the stem. The roots grow longer. They go deep in the ground. The big plant grows flowers. The flowers make seeds. A new seed falls into the soft soil. What will happen next?Title (Slide 0): "Digging Deeper: The Truth About Tillage" Subtitle: How turning the soil affects plants, microbes, and the planet Slide 1: What Is Tillage? Tilling the soil means digging, turning, and loosening it using tools or machines. It's a common farming practice to prepare the land before planting. Slide 2: Why Do Farmers Till? Tillage is usually done before planting to: ⢠Soften and aerate the soil ⢠Mix in nutrients ⢠Remove weeds ⢠Bury crop residues for decomposition and fertility Slide 3: Tools Used for Tillage Farmers use tools like: ⢠Ploughs: Cut deep into the soil ⢠Harrows: Break up clumps and smooth the surface Slide 4: Ploughs vs. Harrows ⢠Ploughs: Used first, go deep, lift and flip soil ⢠Harrows: Used after ploughs, work on the surface to break clumps and level the soil Slide 5: Types of Tillage Systems From most to least soil disturbance: ⢠Conventional Tillage: Deep ploughing ⢠Minimum Tillage: Light disturbance ⢠Conservation Tillage: Only disturb seed zone, keep residues on top ⢠Zero Tillage (No-Till): Plant directly into undisturbed soil Slide 6: Problem 1 â Soil Erosion Tillage removes protective cover, exposing soil to wind and rain. Result: topsoilâthe most fertile layerâis easily washed or blown away. Slide 7: Problem 2 â Disruption of Soil Life Soil is a living ecosystem! ⢠Worms, fungi, and bacteria help aerate soil and release nutrients ⢠Tillage destroys their habitat, reducing fertility and soil health Slide 8: Problem 3 â Loss of Soil Structure Healthy soil has pores for air, water, and roots. Tillage breaks the sponge-like structure, and soil compacts over timeâlike flattening it into a pancake. Hard soil = poor plant growth. Slide 9: Problem 4 â Decreased Organic Matter Microbes "eat" organic matter through aerobic respiration (using Oâ and releasing COâ). Tillage adds oxygen, microbes speed up, and burn through the soilâs âpantryâ of organic matterâleaving it empty and poor. Slide 10: Problem 5 â Greenhouse Gas Emissions Faster decomposition = more COâ released. Tillage boosts microbial activity, which increases carbon dioxide emissionsâcontributing to climate change. â
Conclusion (Slide 11): đą Tillage: A Double-Edged Tool Tillage can help prepare the soil and control weedsâbut it comes at a cost. Over time, repeated tilling can strip away organic matter, destroy soil life, and release greenhouse gases. It's like spending all your savings for quick resultsâand being left with nothing for the future. The smarter path? Use reduced or no-till methods that protect soil health, keep carbon in the ground, and support long-term farming success.The following days are a jumble of gunfire, digging, gobbled food, soldiers running in and out of the forest in small groups, distant explosions, stray shells, bandaged heads and unexpected lulls. On the very first day, before dawn, I am ordered into one of the newly dug trenches. I huddle there, squeezing my magic buttons and singing songs to the dog. When the fighting stops, the dog disappears, but a new companion takes his place. A strange little soldier crawls along the trench toward me. âPrivate Sasha!â he cries. âIâve been looking for you all day long!â Heâs old, like a grandfather, a dedushka. He has a black patch over one eye, a tape measure around his neck and a row of pins threaded into his sleeve. Hanging from his belt is the most enormous pair of scissors I have ever seen and I wonder if he uses them as a weapon. He doesnât tell me his name, so in my head he becomes Dedushka. Dedushka squats, cups his hand to his ear, peers over the top of the trench and smiles. âItâs safe to be upright . . . for now.â He helps me to my feet, dusts me off and commands me to stand as tall and straight as I can. Then he measures me. Everything from head to toe â even my toes! He writes numbers in a little notebook, strings his tape measure back around his neck, salutes and hurries away. Itâs all very strange, and I wonder if Dedushka has been bumped on the head during the battle and is now a little bit muddled. I should have given him a hug before he left. I chase after him but stop when Iâm hit by a shovelful of flying dirt. Sleepy Bear is digging a cave! âAre you going to hibernate?â I ask. Sleepy Bear chuckles. âNo, although that would be wonderful! I could do with a lo-o-o-ong sleep.â He sighs and closes his eyes. He doesnât open them again and I realise that he has gone to sleep. Standing up! I shake his arm, and he opens his eyes and keeps talking. âNo, Iâm not hibernating. Iâm digging a little nook where I can sleep and eat. Iâll hang up my raincape as a door that can open and close so it feels just like a real home . . . except for the lice . . . and the bad smells . . . and the bombs that make the walls shake and crumble.â He points further along the trench to where other soldiers are digging. âWeâre all making little houses in the ground.â âLike rabbits and moles,â I say. Sleepy Bear chuckles. âYes! And soldiers who need to hide from German bullets and bombs.â He stops digging to roll a cigarette. âShould I be making a house?â I ask. âI want to hide from German bullets and bombs, too.â Sleepy Bear flops to the ground, lights his cigarette, closes his eyes and takes a deep puff. I wait for him to answer, but, instead, he begins to snore! I poke him in the side. He snorts and he murmurs, âI think someone has already built you a house, Sasha. Keep going along this beautiful village street and you are sure to find it.â He falls asleep once more. I kiss his dusty cheek and whisper, âThank you, Sleepy Bear.â A little way along, I see Cook in a cloud of smoke. He has lit a fire, right here in the middle of the trench, and is stirring a cauldron full of kasha. He squats as he stirs. âWhat are you doing?â I ask. âCooking supper, of course!â he cries. âBut why are you doing it here?â Cook points his spoon at the ground above the trenches. âBecause if I do it up there, my pot will be filled with holes from German bullets and all of the kasha will leak out onto the ground. Itâs bad enough that our supplies canât get through German lines and thereâs nothing to cook but buckwheat for kasha. But if we lost the kasha, too . . .â âHungry soldiers,â I say. Cook nods. âAnd grumpy!â âLike Boris!â I gasp. âEven worse,â warns Cook. I picture the kasha pot full of bullet holes. And then I realise that if the kasha pot were full of holes, then Cook would be, too. I wrap my arms around Cookâs neck and say, âI think this is a very good place for cooking our supper.â I kiss his smoky cheek and run along. At the end of the trench, I find the biggest hole of all. Itâs wide and deep and as busy as a beehive in a blossom tree. Above, a group of soldiers is rolling logs into place for a roof, while below, typewriters rattle and pencils scratch and papers flutter and voices crackle out of five different radios. Their words tangle together to tell a strange wartime fairy tale about German guns and a loving father called Stalin and a Red Army regiment that is lost in the deep, dark forest and a wicked beast called Hitler and a delivery of vegetables that was hit by a bomb and blown into a million tiny pieces too small even to make soup. In the middle of it all, wrestling with a rumpled map, his rifle still slung over his shoulder, is Major Scruff. âMajor Scruff!â I run and jump into his arms. âIs this our new home?â âYes, Sasha. I suppose it is.â âIs it safe from German bullets and bombs?â I ask. He stares at me. âWere you scared in the trenches today, Sasha?â âNo,â I reply. âI had magic buttons and a dog and some songs to sing. Were you scared in the forest, Major Scruff?â âYes,â he says. âPoor Major Scruff!â I press my hand against his cheek. The dark, rough stubble is grubby with grit and his eyelids are taking a long time to open after every blink. âYou need a shave and a nap!â I scold. He chuckles. âI am too tired to shave and too busy to nap.â I scrunch my nose while I consider his problem. âI know!â I cry. âYou nap and I will shave your whiskers. That will be two jobs tumbled into one!â And so thatâs what we do. Major Scruff slumps into a chair and snoozes while I lather his face with soapy water and shave his whiskers. The soap suds travel from his face, up into his hair and down the front of his uniform, and I have to shave his jaw and chin three times because I keep missing bits, but I finally get it all done. I am just wiping his cheeks dry when the dog appears. He licks my hand, then stretches up and licks soap suds from Major Scruffâs ear. Major Scruff wakes with a start. He feels his newly shaved face and cries, âWonderful, Sasha! I feel smooth, clean, rested and ready for action.â He ruffles my hair. âWe must do this again tomorrow. Although next time, you might wake me with a gentle shake of the shoulder instead of licking my ear.âTypes of Marinades Pineapple Marinade - http://bbq.about.com/od/marinaderecipes/tp/Top-10- Pork-Marinade-Recipes.htm This sweet, fruity marinade works great on any cut of pork or chicken. What you get with this marinade is a great Hawaiian Teriyaki flavor. Try this marinade when you are simply placing cut strips of pork or chicken over rice. You can make extra marinade to use as a sauce as long as you keep it separate from the meat LM-Cookery Grade 10 Pork Chop Marinade This is a great Asian style marinade that works well on all cuts of pork, particularly pork chops, reminiscent of a Teriyaki marinade with a hint of heat from the chili sauce. You can, if you like, heat this up with some extra chili sauce or perhaps a pinch of cayenne. Jamaican Jerk Marinade You've heard of Jerk seasonings and Jerk rubs, well this is a jerk marinade that gets that jerk flavor deep into the meat. You can use this marinade on all kinds of meat and poultry. Pork Rib Marinade BBQ Guru posted this marinade recipe to the forum. It uses a pork rub for the seasoning with vinegar and water to turn it into a marinade. Teriyaki Marinade Want to get that great Teriyaki flavor into your favorite dish? This marinade will surely add flavor to whatever you're grilling. This marinade works particularly well with pork and poultry. Pork Chop and Tenderloin Marinade Doug Freeman sent in this marinade recipe for grilled pork. You may leave out the liquid smoke if you are so inclined. Bourbon Marinade This is a great, sweet bourbon marinade that works perfectly on any food. This is a mild marinade so you will want several hours marinating time with it before you grill. Mustard-Vinegar Marinade This is a simple mustard marinade that tenderizes and adds flavor. It works well on pork or poultry.A. The continental plate remains above, while the oceanic plate subducts. The older and denser oceanic plate subducts beneath the younger plate. A subduction is the process by which an oceanic plate slide under a less dense plate, can be a continental or another oceanic plate. In this process, the plates involved are oceanic plate and continental plate. Oceanic Plate is thinner plate, Dense,generally, slides under into the mantle; and especially when it is older than the other oceanic plate. They may slide over given that it is the younger oceanic plate in the oceanic-oceanic subduction. In case of oceanic-continental subduction, even younger oceanic plate can never slide over it. Continental Plate is thicker plate, less dense and slides over and experiences compression and volcanic activity. Another concept is about buoyancy. Consider the Earthâs mantle as a giant swimming pool. Floating on top of it are the Earth's tectonic platesâsome thin and dense, like the oceanic crust, and others thick and less dense, like the continental crust. Imagine the thin oceanic plate and the thick continental crusts are like tennis ball and soccer ball, respectively. When placed in water, the tennis ball sinks at the bottom and easily subducted as it is smaller and denser. Contrary, the soccer ball is larger and more buoyant, thus, resists subduction and tends to stay afloat. Therefore, during subduction, the thin and dense oceanic crust or an older oceanic crust slide under another plate due to its low buoyancy. Consequently, the thick and denser continental plate or younger oceanic plate slides over because of its high buoyancy. In the subduction zone, there are two landforms that are formed in the process, namely, trench and volcanic arcs. Trenches are deep valleys formed at the edges of the colliding plates, where an oceanic plate bends downward and starts to subduct another plate. It looks like a long, narrow depression where marks the zone where subduction begins. The other landform is the volcanic arc, a chain of volcanoes that formed on the overriding plates where water and sediments from the sinking slab cause the mantle wedge above it to melt, making the magma rise to the surface and forming the volcanoes. a. The formation of trench When these two plates collide, the oceanic plate is subducted and pulled into the mantle. The edges of the plates create a deep valley which we call trench. b. Formation of volcanic arcs When a denser oceanic plate collides with a less dense continental plate, oceanic plate is subducted and pulled into the mantle. As it reaches the mantle, the plate is subjected to extremely high pressure and temperature. This causes the trapped water and air in the plate to be released. The plate eventually melted back as magma. The formed magma rises to the surface. This gives rise to the formation of volcanic arcs. The same is true between the collision of two oceanic crusts as the older crust is subducted over the younger crust. However, the collision of two continental crusts will not result in the formation of trenches.